Lehnerite is a rare secondary phosphate mineral typically found as small, vibrant yellow tabular crystals within weathered pegmatite deposits. It is specifically recognized for its occurrence in phosphate-rich zones of granite pegmatites and requires careful handling due to its uranium content.
Is this lehnerite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch lehnerite with a known reference. Lehnerite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to resinous.
- 4Match the color rangeCompare against the expected color range: bronze, honey yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, radial aggregates.
Often confused with
Lehnerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside lehnerite
Minerals reported to co-occur with lehnerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn²⁺(UO₂)₂(PO₄)₂·8H₂O
- Mohs hardness
- 2-3
- Density
- 3.5-3.6 g/cm³
- Colors
- Streak
- Pale yellow
- Luster
- Vitreous to resinous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals, radial aggregates
- Cleavage
- Perfect on {010}; good on {101}; less good on {101}; poor on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral in the oxidized zone of a complex granite pegmatite
Where rockhounds find lehnerite
Classic worldwide localities
- Hagendorf, Bavaria, Germany
Field-hunting tip
Where it forms: A rare secondary mineral in the oxidized zone of a complex granite pegmatite. If you start seeing zwieselite, rockbridgeite in float, you are in the right ground. Typical habit: tabular crystals, radial aggregates. Train your eye for that shape before scanning the outcrop.





